Non-volcanic passive margins
Код 3302524
- ISBN: 978-5-5146-5358-4
Код 3302524
High Quality Content by WIKIPEDIA articles! Non-volcanic passive margins (NVPM) constitute one end member of the transitional crustal types that lie beneath passive continental margins; the other end member being volcanic passive margins (VPM). Transitional crust welds continental crust to oceanic crust along the lines of continental break-up. Both VPM and NVPM form during rifting, when a continent rifts to form a new ocean basin. NVPM are different from VPM because of a lack of volcanism....
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